沙特阿拉伯上二叠纪Khuff组石灰岩中保存异常完好的二叠石cf. tenellus (Pia)(裸子科)

IF 4.1 3区 地球科学 Q1 PALEONTOLOGY Journal of Micropalaeontology Pub Date : 2017-04-27 DOI:10.1144/jmpaleo2016-005
G. Hughes
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引用次数: 2

摘要

与1955年的P. tenellus sensu Elliott相比,沙特阿拉伯Khuff组的上二叠世细粒石灰岩中描述了一种保存异常完好的关节红藻二叠石标本。纵向髓质和束状皮质细丝通过一系列长球状、凹或凸终止、互锁的节段延伸,它们被解释为在关节中起作用。花丝倾向于向外伸展并向皮层分支,在皮层的气孔处终止。在顶孔处,花丝伸展为分叉分支,也可能是三叉分支,并可能作为新节的起源。外髓质发育了许多细长的球状室,每排最多5个,与丝密切相关,被认为是生殖孢子囊。该标本被认为主要处于低能量、正常到略高盐度、泻湖潮下状态下的浅层环境中。
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Exceptionally well-preserved Permocalculus cf. tenellus (Pia) (Gymnocodiaceae) from Upper Permian Khuff Formation limestones, Saudi Arabia
An exceptionally well-preserved specimen of the articulated rhodophyte Permocalculus, compared with P. tenellus sensu Elliott, 1955, is described from fine-grained Upper Permian limestones of the Khuff Formation of Saudi Arabia. Longitudinal medullary and sheaf-like cortical filaments extend through the uniserial series of elongate-globular, concave- and convex-terminating, interlocking segments for which they are interpreted to have functioned in articulation. The filaments tend to splay and branch laterally into the cortex where they terminate at the pores. At the terminal aperture, the filaments extend as bifurcating and possibly trifurcating branches and may serve as the origin of a new segment. Numerous elongate-globular chambers, up to five in each row and intimately involved with the filaments, are developed in the outer medulla and are considered to represent reproductive sporangia. The specimen is considered to have occupied predominantly low-energy, normal to slightly elevated salinity, shallow conditions within the subtidal regime of a lagoon.
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来源期刊
Journal of Micropalaeontology
Journal of Micropalaeontology 生物-古生物学
CiteScore
4.30
自引率
5.00%
发文量
7
审稿时长
>12 weeks
期刊介绍: The Journal of Micropalaeontology (JM) is an established international journal covering all aspects of microfossils and their application to both applied studies and basic research. In particular we welcome submissions relating to microfossils and their application to palaeoceanography, palaeoclimatology, palaeobiology, evolution, taxonomy, environmental change and molecular phylogeny.
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